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Sexlingar Farmhouse and Orchard <br />Resldentlal Development Project <br />CEQA Findings <br />would be replaced with trees matching the existing type, arrangement, pattern, and shape <br />of the orchard within Lot 1. This would retain the feeling, appearance, and character of <br />the historical resource in this portion of the project site. (January 2014 EIR Attachment, <br />p. 5) However, while the project would preserve the residence, garage, and portion of <br />the orange trees, the property would be transformed from a historic single family <br />residence and orchard to a suburban development with a small orchard and 22 new <br />single - family residences. (January 2014 EIR Attachment, pp. 5 -6.) <br />However, because the property would retain many of its major elements and still convey <br />the significance of a property type once common in the City, and because the historic <br />structures will be surrounded by compatible low density residential use, the property's <br />location, feeling, and overall character will be maintained. Therefore the project will <br />meet Secretary of Interior Standards for the Treatment of Historic Properties, reducing <br />any potential for impacts to less than significant. (January 2014 EIR Attachment, p. 5 -6; <br />Cultural Resources Technical Memorandum, URS (November 2013)) <br />D. GEOLOGY AND SOILS <br />1. Impact: Would the project be located on a geologic unit or soil that is unstable, or that <br />would become unstable as a result of the project, and potentially result in on- or off -site <br />landslide, lateral spreading, subsidence, liquefaction or collapse? <br />Finding: Less Than Significant. (EIR, pp. 5 -44, 5 -45; January 2014 EIR Attachment, p. <br />6.) <br />Analysis: According to the California Department of Water Resources, the depth to <br />groundwater in the project area is more than 50 feet. Liquefaction potential is considered <br />negligible due to the relatively cohesive and dense nature of the underlying materials and <br />lack of a shallow groundwater table. No evidence of past landslides or slope instabilities <br />has been observed. Liquefaction is not generally considered to be a hazard if the water <br />table is deeper than 50 feet, Thus, there is low probability for liquefaction, subsidence <br />and landslides. Due to the site's elevation and distance from any open bodies of water, <br />potential for seiehe is also negligible. Therefore, any impact is considered less than <br />significant. (EIR, p. 4 -44, 4 -45; January 2014 EIR Attachment, p. 6.) <br />2. Impact: Would the project be located on expansive soil, as defined in Table 18 -1 of the <br />Uniform Building Code, creating substantial risks to life or property ?? <br />Finding: Less Than Significant. (EIR, pp. 5 -44, 5 -45; January 2014 EIR Attachment, p. <br />6.) <br />Analysis: The project site consists of Quaternary -age alluvium consisting of silty sand <br />and sandy silt materials which at depth change to dense gravelly sand. Based on <br />laboratory testing with similar soils, the materials on the project site possess a very low <br />expansion potential. Thus, impacts are less than significant. (EIR, p. 4 -44, 4 -45; January <br />2014 EIR Attachment, p. 6.) <br />12 "Exhibit A" <br />